Tracking Magma‐Crust‐Fluid Interactions at High Temporal Resolution: Oxygen Isotopes in Young Silicic Magmas of the Taupō Volcanic Zone-Reference-Cited by-同舟云学术

Tracking Magma‐Crust‐Fluid Interactions at High Temporal Resolution: Oxygen Isotopes in Young Silicic Magmas of the Taupō Volcanic Zone

Published:2023-01 Issue:1 Volume:24 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Rooyakkers Shane M.¹^ORCID,Faure Kevin¹,Chambefort Isabelle²,Barker Simon J.³^ORCID,Elms Hannah C.³,Wilson Colin J. N.³^ORCID,Charlier Bruce L. A.³

Affiliation:

1. National Isotope Centre GNS Science Lower Hutt New Zealand

2. Wairakei Research Centre GNS Science Taupō New Zealand

3. School of Geography, Environment and Earth Sciences Victoria University of Wellington Wellington New Zealand

Funder

Ministry of Business, Innovation and Employment

Royal Society Te Apārangi

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010694

Reference128 articles.

1. Absar A. &Blattner P.(1985).Successive hydrothermal events as indicated by oxygen isotope composition and petrography of greywacke basement rocks Kawerau geothermal field New Zealand. InProceedings 7th New Zealand Geothermal Workshop Auckland New Zealand(pp.115–122).

2. A cascade of magmatic events during the assembly and eruption of a super-sized magma body

3. From mush to eruption in centuries: assembly of the super-sized Oruanui magma body

4. The invisible hand: Tectonic triggering and modulation of a rhyolitic supereruption

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